Submerged or partially submerged sea caves
Sea caves are formed where the specific geology of an area allows for the weathering and erosion of material to create overhangs, clefts, caves and tunnels that provide very specialised conditions for marine animals and plants.
The UK has the most varied and extensive sea caves on the Atlantic coast of Europe.
Within the SAC, sea caves are present around Pen Llŷn including the Tudwal Islands and also along the Merionnydd coast north of Tonfannau and the Ceredigion coast north of Clarach. A wide variety of cave types are present with differing morphology and exposed to varying degrees of wave action, tidal streams and scour from sand suspended in the water and stones/rocks on the cave floors. The geology of the SAC is complex and the variety of rock types and other geological features such as folding, fracturing and faulting and erosion have provided the basis for the formation and variety of sea caves within the site.
Sea cave communities range from scoured sparse communities characterised by lichens, red seaweed (such as the sand-binding seaweed Audouinella purpurea) and molluscs grazing on biotic films (e.g. at Porth Towyn, Trwyn Cilan, Black Rock, Rhoslefain, and Clarach) to a variety of communities that are rich in seaweed species, sponges, anthozoans (sea anemones and relatives) and ascidians (sea squirts) (e.g. at Porth Llanllawen NE of Bardsey Sound, Ogof Deuddrws at Aberdaron, and East St Tudwal’s Island).